Continental Boundaries: The shape and location of continents play a significant role in determining the path of ocean currents. Large landmasses can deflect currents and create unique circulation patterns.
Ocean currents can be broadly classified into two main types: surface currents and deep currents.
Surface Currents: These currents are driven primarily by wind and are located in the top 400 meters of the ocean. They play a crucial role in distributing heat around the globe and can have a significant impact on regional climates.
Deep Currents: Also known as thermohaline currents, these currents are driven by differences in waterdensity, which are influenced by temperature and salinity. Deep currents can circulate water throughout the ocean basins, playing a key role in the global conveyer belt of oceancirculation.
By mastering these concepts, you will gain a comprehensive understanding of oceancirculation and its significance in the broader context of Earth's systems.
[Ocean Circulation] Related Worksheets and Study Guides:
Identify and analyze forces responsible for changes in rotational motion and develop an understanding of the effect of rotational inertia on the motion of a rotating object (e.g., merry-go-round, spinning toy, spinning figure skater, stellar collapse [supernova], rapidly spinning pulsar).